89 results were found for [77AGG. COM]pjo slot nos4d slot ok jp slot diana slot oja89 slot axis slot pe3.

Results:

• 11. Kriauciuniene_Jurate_CES_2010

  Regional temperature, precipitation and runoff series in the Baltic countries Jurate Kriauciuniene1, Alvina Reihan2, Tanya Kolcova3, Diana Meilutyte- Barauskiene1, Lita Lizuma3 1 Lithuanian Energy Institute, 2Institute of Environmental Engineering, Tallinn University of Technology, 3Latvian Environment, Geology and Meteorology Centre Outline boxshadowdwnboxshadowdwn Purposes of the study /media/ces/Kriauciuniene_Jurate_CES_2010.pdf

• 12. Ice subsidence above eastern Skaftá cauldron

  This graph shows the ice-surface lowering (subsidence) of the eastern Skaftá ice-cauldron in Vatnajökull ice cap in October 2015. Vertical displacement (m) was monitored by near real time presentation of data from a GPS station, mounted in the middle of the cauldron. The maximum elevation above sea level, top left (hæð), refers to the zero value on the y-axis; while such value top right /hydrology/research/skafta-cauldron/

• 13. Gradual fading of seismic activity at Bárðarbunga and the dyke intrusion

  of events of magnitudes M1-2 (blue), M2-3 (green) and M>3 (red). Both lower panels show the activity on the caldera rim, moment on the left and event numbers on the right, here the colours for the event numbers are M3-4 (blue), M4-5 (green) and M>5 (red). Please notice that the last data point in all plots represents the ongoing week and might thus still change. Further, the y-scale is logarithmic /earthquakes-and-volcanism/articles/nr/3039

• 14. VI_2009_013

  to locate earthquakes in Iceland but the SIL-crustal model has no Moho boundary. Using this model in the routine, daily analysis, the majority of the earthquakes in Eyjafjallajökull form a 3-km-wide chimney between 1 and 10 km depth beneath the northern flank of the volcano. A smaller cloud is also visible between 19 and 25 km depth, about 1.5 km west of the main activity/cluster. 13 Figure 3 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 15. Grimsvotn_status_2011-05-24_IES_IMO

  and around it. The estimated height is below 5 km since clouds over the glacier were at 5-7 km and the plume did not reach above the cloud deck. The ash plume reached 8 km briefly at 14 UTC today, but decreased shortly there after. According to pilot reports the plume is visible at around 10 thousand feet, mostly light gray or brown in color, but pulsating to 15 thousand feet /media/jar/Grimsvotn_status_2011-05-24_IES_IMO.pdf

• 16. VI_2019_009

  26 36 40 41 46 50 51 52 53 54 58 60 61 62 63 64 65 68 70 71 72 73 74 80 81 83 84 85 86 87 92 Present weather (Manual) Present weather ( Automatic ) Number of records a71 a71 a71 250 500 750 250 500 750 Number of records Figure 15. Automatic station as a function of manual station. a71 a71a71a71a71a71 a71a71 a71a71a71 a71a71 a71 a71 a71a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71a71a71 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 17. Journal_of_Hydrology_Veijalainen_etal

  A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 18. Paper-Olafur-Rognvaldsson_92

  for Meteorological Research, Reykjavík, Iceland 5Bergen School of Meteorology, Geophysical Insitute, University of Bergen, Norway †Corresponding author: or@belgingur.is, Orkugarður, Grensásvegur 9, 108 Reykjavík ABSTRACT Atmospheric flow over Iceland has been simulated for the period Jan- uary 1961 to July 2006, using the mesoscale MM5 model driven by initial and boundary data from the ECMWF. Firstly /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 19. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 20. FMI_-_Disaster_Mitigation

  Disaster Mitigation Kevin M. Simmons, Ph.D. Austin College Fulbright Research Scholar International Centre for Geohazards Oslo, Norway Economic and Societal Impacts of Tornadoes By Kevin M. Simmons and Daniel Sutter © 2010, 296 pages in paperback ISBN: 978-1-878220-99-8 AVAILABLE NOVEMBER 2010 from the American Meteorological Society and the University of Chicago Press Research Agenda /media/loftslag/FMI_-_Disaster_Mitigation.pdf